new evidence on the uruk expansion in central mesopotamia
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New Evidence on the Uruk Expansion in CentralMesopotamia
Regis Vallet, Johnny Baldi
To cite this version:Regis Vallet, Johnny Baldi. New Evidence on the Uruk Expansion in Central Mesopotamia. Paléori-ent, CNRS, 2017. �hal-03088138�
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017 Manuscrit reçu le 28 juillet 2016, accepté le 15 décembre 2016
New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont
R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Abstract: The new data from the sites of Girdi Qala and Logardan (Iraqi Kurdistan) are starting to change the picture of Uruk culture expansion. In the Central Zagros Piedmont, it began as early as the second half of the local Late Chalcolithic 2 (LC2), contemporary with South Mesopotamian Early Uruk. The Uruk presence is documented not only by a large ceramic assemblage, characterized by a broad range of shapes and techniques, but also by numerous production facilities which show that Uruk pottery was made on-site by resident craftsmen. These discoveries lead us to revise traditional conceptions of the Uruk expansion, based on the simple dichotomy between local populations and Uruk colonists. We can now assess the actual forms of intercultural exchange that were taking place over an unexpectedly long period of time.
Résumé : Les nouvelles données provenant des sites de Girdi Qala et Logardan (Kurdistan d’Irak) commencent à offrir une image renouvelée de l’expansion de la culture d’Uruk, qui débute, dans le piémont mésopotamien du Zagros central, dès la seconde moitié du Chalcolithique récent 2 local (LC2), contemporain de l’Uruk ancien du Sud mésopotamien. La présence urukienne est documentée non seulement par un vaste assemblage céramique, caractérisé par une grande diversité de formes et de techniques, mais aussi par de nombreuses installations de production, démontrant que la poterie Uruk était fabriquée sur place, par des artisans installés à demeure. Ces découvertes amènent à nuancer les conceptions traditionnelles de l’expansion urukienne, fondées sur une dichotomie élémentaire entre populations locales et colons urukiens, si l’on veut apprécier les modalités précises d’échanges interculturels s’inscrivant dans une durée insoupçonnée.
Keywords: Iraqi Kurdistan; Mesopotamia; Qara Dagh; Uruk expansion; Late Chalcolithic; Ceramic technology. Mots-clés : Kurdistan d’Iraq ; Mésopotamie ; Qara Dagh ; Expansion de la culture d’Uruk ; Chalcolithique récent ; Technologie céramique.
INTRODUCTION
Excavation on the sites of Girdi Qala and Logardan, west
of the Qara Dagh range in Chamchamal District (Sulaymaniyah
Governorate) in Iraqi Kurdistan, started in 2015 with three
weeks of fieldwork (6-27 October)1. The scientific purpose of
this new project is to study the formation of complex societies,
1. The project, under the responsibility of Régis Vallet, gathered 15 research-
ers and engineers from France, Belgium, Italy and Iraq. It is funded and
supported by several institutions, mainly, in France, the Commission
des fouilles (Excavations committee) of the Ministry of Foreign Affairs
(MAEDI), and in Belgium the University of Liège, but also the CNRS, the
University of Paris 1 and the IFPO.
the appearance of territorial polities and long-term intercul-
tural processes. Indeed, despite recent developments (Kopanias
and MacGinnis 2016), Southern Kurdistan remains poorly
documented, although it seems an ideal laboratory for investi-
gating these research questions. It is no exaggeration to say that
the region is at the very heart of the Near East, a crossroad
between Northern and Southern Mesopotamia as well as
between Mesopotamia and Iran (fig. 1). The project more spe-
cifically focused on the Chalcolithic period, following on from
our previous work at both ends of the Fertile Crescent, at Tell
el ‘Oueili in Southern Iraq (Huot et Vallet 1990; Vallet 1990
and 1996) and Tell Feres in Northern Syria (Forest et al. 2014;
Vallet 2014 and in press; Vallet and Baldi 2016), and on the
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62 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
Bronze age, two periods for which the redefinition of cultures
on a regional basis is a major issue.
The main goal of the first campaign was to begin to estab-
lish the sequence of the sites, by excavating well preserved in situ levels. At both sites we opened three trenches (A, B and
C), of 10 x 5 m. We shall only present here the trenches that
provided Chalcolithic remains.2 The Uruk presence is docu-
2. At Girdi Qala, Trench A, under the responsibility of Dominique Parayre
(University of Lille 3) and Martin Sauvage (CNRS), was set to test the
upper levels of the main mound and the possibility of an extensive exca-
vation of its flat summit, while the operation in Trench B, conducted by
L. Colonna d’Istria (University of Liège), at the opposite side of the hilltop,
had a stratigraphic purpose. They encountered Hellenistic, Sasanian and
Islamic levels (forthcoming report).
mented by a series of features that excavations are just starting
to reveal: a large craft area in Trench C at Girdi Qala and a
stone ramp at Logardan (Trenches A and B). Moreover, the
settlement located on a secondary north mound at Girdi Qala
is still unexcavated, but the pottery identified during the sur-
face collection belongs exclusively to Southern Uruk traditions
and is characterized by a low rate of fragmentation (Orton
1993). It could suggest the presence of an Uruk enclave aban-
doned even before the end of the Late Chalcolithic, with little
disturbed contexts. Likewise, the understanding of the Uruk
presence at Logardan requires the identification of larger and
well-stratified evidence. But the presence of the stone ramp (as
well as its chronology) offers a glimpse of the degree of social
organization and integration between local inhabitants and
Uzyam Dam
Hamrin DamQadissiya Dam
Dukan Dam
Bakhma DamHasakah Dams
Middle Khabur Dam
Cizre Dam
Eski Mosul Dam
Makhul Dam
Ilusu Dam
Darbandikhan Dam
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MM
s40° 42° 44° 46°
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0 100 200 km
metres
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© Qara Dagh Archaeological MissionMap : Martin Sauvage (CNRS, USR 3225, Nanterre, France)
AL-ANBAR DIYALA
ARBIL
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AT TA'MĪM
AS SULAYMANIYAH
SALAH AD-DIN
Euphrates
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abTigris
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S Y R I A
I R A Q
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Tharthar Lake
LogardanGirdi QalaDayr az-Zawr
Al Qamishli
Al Hasakah
Urmia
MosulArbil
As SulaymaniyahChamchamal
Baghdad
Kirkuk
Fig. 1 – Geographical location of Girdi Qala and Logardan, Northern Iraq.
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 63
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
southern settlers. In other words, in the coming years, the
archaeological record from Girdi Qala and Logardan will
enable us to re-open the debate on Late Chalcolithic–Uruk
‘culture-contact’.
CULTURE CONTACTS IN THE URUK PHASE
In the archaeological literature on late prehistoric
Mesopotamia, the relations between the northern and south-
ern part of the region have always been examined with a spe-
cial attention. In particular during the 1990s and the first half
of the 2000s, many archaeological studies and reflections have
stressed differences, parallelisms and connections between
North Mesopotamian Late Chalcolithic polities and Southern
Uruk proto-cities (Rothman 1993 and 2001; Rothman and
Peasnall 1999; Stein 1999; 2001 and 2002a; Gut 2002; Postgate
2002). This dynamic was mainly fueled by new information
about northern proto-urban centers (especially Tell Brak and
Arslantepe: Oates and Oates 1993; Frangipane 1993; 1996;
2000; 2001 and 2002), as well as by reassessment of ancient
excavations (as Nineveh and Tepe Gawra: Gut 1995 and 2002;
Rothman 2002). Data from Southern Anatolia and Northern
Syria were clearly showing that Northern Mesopotamia has
been the center of an independent proto-urban development as
old as the southern one. As a consequence, the debate focused
both on dynamics and chrono-cultural issues of North–South
relations (Marro et Hauptmann 2000). On the one hand,
micro-scale approaches have been applied at specific sites
(especially at Hacınebi: Stein 2001 and 2002a-b)3 as mirror of
a wide complex organization; whereas the large-scale per-
spective of Wallerstein’s (1974 and 1980) theory of the “World
System” has provided a main interpretative outlook since the
1990s (Algaze 1993; Stein 1999). On the other hand, the adop-
tion of the Santa Fe chronological chart (based on the Late
Chalcolithic periodization: Rothman 2001) clarified several
cultural and terminological misperceptions, largely due to
the fluid (and inappropriate) definition of ‘Northern Uruk’
to indicate the phase of culture contact. However, since the
reassessment carried out by P. Butterlin (2003), discussions
have virtually ceased. Ever since the paradigmatic model of
Greek expansion in the Mediterranean was proposed (Stein
2002b) and the idea of political expansion revised in favour
of economic and trade models (Stein 1998; Algaze 1999),
3. In this sense, the thematic issue on the Uruk expansion in Paléorient, vol. 25.1 (1999), with its large discussions about Hacınebi and the Uruk
colonial sphere, marked a focal moment of the archaeological debate.
no further theoretical arguments have emerged to feed the
debate.
The same reasons that had awakened interest in North-
South relations—namely increasing evidence for a highly
structured social complexity in the North—gradually pushed
attention towards indigenous northern dynamics (al-Kountar
and Reichel 2008; Reichel 2009; Frangipane 2009 and 2010).
At the same time, since the new data mainly concerned north-
ern polities, the interpretive schemes about the Uruk network
and settlements remained quite stable. Despite the biased
character of the available data on the Uruk expansion—almost
exclusively limited to the Euphrates basin—general explana-
tory models have not evolved (Badler 2002; Habibi and
Karami 2008-2009). Indeed, scholars had noticed the unsatis-
factory nature of theories based on a too incomplete record
(Butterlin 2003; Reichel 2008-2009), but they did not have
sufficient information to suggest alternative hypotheses.
Actually, despite many re-evaluations of the theoretical
schemes based on a core-periphery dichotomy, the Uruk
expansion is still often conceived (Eichmann 1991 and 2007;
Goulder 2010; Gopnik and Rothman 2011) as a dynamic
between a dominant area (the South, with focus on highly
skilled intensive production) and a marginal zone (the North,
with focus on low skilled extraction and production of raw
materials). Indeed, as regards the so-called Uruk colonial
expansion, solid archaeological evidence exists in the North
for the second half of the 4th millennium BC (Late Chalcolithic
[hereafter LC] LC4-5 phases), with the foundation of main
colonies as Habuba Kabira, Jebel Aruda, Brak TW 12,
Jarablus Tahtani or Hassek Höyük (Strommenger 1980;
Strommenger et al. 2014; Van Driel and Van Driel-Murrey
1979; Van Driel 1980; Oates and Oates 1993; Vallet 1997a-b
and 1998; Stephen and Peltenburg 2002; Helwing 2002;
Forest and Vallet 2008).4 But for the first stages of the Uruk
expansion in the North, current knowledge is restricted to the
settlement of Sheik Hassan (Boese 1995; Bachmann 1998a-b)
and to some southern enclaves within northern villages (as at
Hacınebi, Samsat or el-Kowm: Stein 2001; Özguç 1992;
Cauvin et Stordeur 1985).
Obviously, after just one short season of excavations, the
evidence from Western Qara Dagh is still limited and the aim
of this paper is not to use some scattered elements to develop
general theories. The purpose is rather to present and briefly
4. It is never superfluous to stress that, in the same time, the archaeological
record for the South is quite limited. The notion of “Uruk sphere” in itself
is an antonomasia, based essentially on the sounding in the Eanna area
(Nissen 2002).
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64 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
discuss data which contradict some longstanding chronologi-
cal assumptions about the Uruk expansion and shed new light
on the very poorly known topic of craft production within the
Southern Uruk colonial network.
THE SITES
The sites of Girdi Qala and Logardan are located in the
eastern part of the plain of Chamchamal (fig. 2), on the west
bank of the river Tavuq Cay that runs to the south-east, parallel
to the djebel Qara Dagh and then, more to the south, to the
south-west to join the Nahr al Uzaym that flows itself into the
Tigris. The river has many tributaries, mostly on its west bank,
and both sites are built at the junction of two of them, the
Tchachma Spi and the Tawer Hamid (fig. 2). Two brief surveys
of the sites in April 2014 and June 2015 had convinced us of
their scientific potential. According to the surface material that
we were able to identify, Girdi Qala displays a sequence rang-
ing from the LC1 to Islam, and Logardan, less than 1.5 km to
the north, from the Halaf period to the Iron Age. Girdi Qala
(Lat. 35°30’59.10’’N/S – Long. 44°53’00.93’’E/W) is a typical
tabular tell of 15 m high (figs. 3-4) with a diamond-shape flat
top (80 x 70 m; 0.45 ha). The base of the tell covers an area of
approximately 140 m (NS) x 120 m (EO), ca 1.32 ha, but the
site is not limited to the proper tell and extends beyond, par-
ticularly to the south (over a length of 40 m), according to the
topography, the distribution of the surface material (that covers
ca 3.5 ha), the geomagnetic survey and our Trench C. Moreover,
we discovered during the campaign that the site has a northern
extension, 150 m to the north-west, over a secondary low
mound (of ca 200 x 150 m, adding at least 2 ha to the site)
entirely covered by Chalcolithic material (fig. 4). The total
length of the site is about 380 m from the north-west to the
south-east. Logardan (Lat. 35°31’42.17”N/S; Long. 44°52’34.78”
E/W) is quite different (fig. 5). It is not a regular tell. The site
is set on top of a high (27 m) natural hill, roughly triangular in
Fig. 2 – Satellite view of the micro-region around Girdi Qala and Logardan with their respective position and limits.
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 65
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Fig. 3 – Girdi Qala, a view from the southwest.
652.7
645.5
607.3
590.4
638.7
621.2
644.3615.2
Tavuq Çay (Riv.)
Tawer Hamid (Riv.)
588.6
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635
489400 489500 489600 489700
489400489300 489500 489600 489700
3930200
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3930400
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3930500
Trench A
Trench B
Trench C
GIRDI QALA
Surveyed with thedolite LEICA TCR1205and connected to UTM projection, zone 38Elevations got by GPS measurementContours interval: 1 mSuveyed in October 2015 by P. COURBONQARA DAGH Archaeological Mission
0 50 100m
Fig. 4 – Girdi Qala, topographic map.
shape with steep slopes, except to the east where the ground
gently slopes down through three successive terraces (225 x
165 m altogether at the summit of the hill, ca 3.7 ha) that
proved to be partly artificial (fig. 6).
FIRST EVIDENCE OF THE URUK PRESENCE AT LOGARDAN
At Logardan, the main stratigraphic operation (Trench C)
has yielded limited Uruk evidence and much more extensive
remains dating back to Halaf, Early Ubaid and the Bronze
Age. It confirms the results of the surface collection previously
carried on in April 2014 and June 2015.
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66 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
Fig. 5 – Logardan, a view from the west.
Fig. 6 – Logardan, a partial topographic map.
(from Halaf to Late Uruk) were so abundant. The aim was to
clarify the issue of the substratum of the site, rather than to
begin immediately with a time consuming deep sounding at
the top, that would not have given us decisive information in
time. As we thought, the artefacts had slipped down from the
top and the site rests upon a natural hill. At the same time we
discovered a completely unexpected feature: the retaining
stone-wall of a ramp. Some of its stones were visible on the
surface higher to the east, where we placed a second trench
(Trench B). So it turned out that the main goal of both opera-
tions was to clarify dimensions, stratigraphic relationships and
dating of this massive stone structure, clearly inherent to an
important phase of the settlement. Such a construction implies
the use of considerable workforce to provide an access to the
high part of a site. If the top of the hill (a quite restricted space)
deserved a similar investment in terms of time and labor, it was
obviously considered as significant.
The excavation in Trenches A and B has focused on the
retaining wall of a ramp identified on the south-western slope.
Initially, Trench A was conceived as a small test trench on the
south-west flank of the mound, where the Chalcolithic finds
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 67
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According to the South Mesopotamian Uruk sherds col-
lected amongst the stones and in the basal level, the ramp dates
back to the first half of the 4th millennium BC. On the other
hand, on the top of the mound (amongst Halaf, Ubaid, Middle
Bronze and Early-Middle Southern Uruk sherds), a clay Uruk
cone has also been recovered (fig. 7). This very rare kind of
architectural decoration, generally reserved to conspicuous (or
even monumental) buildings, seems to confirm the presence on
the top of the site of important installations, to which the stone
ramp gave access.
Trench A is a 4 x 8 m operation, which enabled us to define
the orientation and size of the retaining wall. It is a 2 m thick
structure composed of uneven rubble stones supporting a
causeway excavated in the virgin soil. In this area, above and
below the ramp, there was no structure and the soil is com-
pletely natural. The retaining stone wall lies on a 3 cm thick
floor. This floor—easily recognizable in section—is made up
of a layer of sherds placed on a hardened hearth deposit. The
whole gently upwards-sloping structure shows traces of mortar
as well as some fragments of unbaked bricks and sherds
between the stones (fig. 8). It is clear that it was built to climb
the hill by arranging non-anthropic levels.
Trench B is a 4 x 7 m operation (figs. 9-10) carried out to
recognize another sector of the ramp. The nature of this struc-
ture is confirmed by the fact that between Trenches A and B
the causeway rises over two meters.5 Dimensions and struc-
tural features of the ramp are identical to the characteristics
observed in Trench A, with mortar, sherds, fragmentary bricks
between stones and a basal floor paved with sherds.
Further east, along the southern slope of the hill, several
stone alignments of the causeway emerge according to a fairly
gentle but uniform slope. The easternmost remains of the
ramp have been identified close to the limit of an anthropic
terrace of the upper town, on the south-eastern slope, where
natural erosion and modern agricultural activities have erased
the causeway. In this sector of the site, the residual stone
blocks were found on some extremely eroded remains of
Halaf constructions, which lied on the virgin soil. It indicates
that, in this area, the retaining wall of the ramp, built to facili-
tate climbing up the natural slopes, had been placed over the
remains of an Early Chalcolithic settlement to give access to
Late Chalcolithic facilities or structures.
Close to this sector, on the south-eastern slope of the hill,
5. The solidity of the retaining wall of the ramp is confirmed by the large
lime furnaces stacked upon and recessed below the causeway during the
Middle Bronze Age, many centuries after the structure had been aban-
doned (fig. 9).
Fig. 7 – Uruk architectural cone found on the top of Logardan.
Fig. 8 – Girdi Qala Trench B. Sherds of bevelled-rim bowls amongst the stones of the 4th millennium ramp.
some slight traces dating back to mid-4th millennium (LC3-LC4
phases) have been identified in the Level 4 of Trench C. Amongst
the phases documented by this operation (from the Early
Chalcolithic to the Bronze Age), Level 4 has yielded a very elu-
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68 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
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sive evidence, with poorly preserved structures and a limited
amount of ceramics (64 Southern Uruk sherds, with just four
diagnostic shapes),6 coming from the heating chambers of two
middle-sized kilns. Both of them belong to the same simple up-
draught typology documented by the majority of the kilns in
Trench C at Girdi Qala (see below). The only value of this very
limited evidence is, therefore, to confirm the existence of a set-
tlement on the top of Logardan in the mid-4th millennium BC.
More generally, it is obvious that, despite the fact that
architectural cones represent a regular element of the Uruk
cultural package (Eichmann 1989; 1991 and 2007; Nissen
6. According to morphology and fabrics of the sherds, local specimens were
virtually absent.
2002; Strommenger et al. 2014), a specimen from a surface
collection is just a suggestive indicator of the possible exis-
tence of a monumental building on the top of the site. In the
same way, the fact that the stone ramp and two kilns (two sec-
ondary depositional contexts) have yielded only Southern Uruk
ceramics cannot in any way be considered as a mark of the
South Mesopotamian identity of the people who built and used
these structures. For the moment, it indicates that South
Mesopotamian-related people were implicated in some degree
in their construction. However, with its well-planned design,
regular layout and massive dimensions, the ramp (fig. 10) pro-
vides evidence for a level of organization and local integration
hitherto unsuspected for Southern Uruk communities settled
in the area during the first half of the 4th millennium BC.
N
Logardan 2015Plan of Trench B
0 1 2 m
Middle Bronze structures
Late Chalcolithic ramp
107
103
101
104
108
106
102
109
105
Fig. 9 – Logardan, plan of Trench B.
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 69
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EXCAVATIONS AT GIRDI QALA TRENCH C: STRATIGRAPHY OF A CRAFT AREA
With the aim of identifying in situ levels dating back to
Chalcolithic times, a 5 x 10 m stratigraphic trench was set up
along the southern slope of the main mound. This choice was
justified by the concentration of Late Chalcolithic ceramic
materials collected in this area during the preliminary surveys
carried out in April 2014 and June 2015.
Indeed, during the first half of the 4th millennium BC, the
south-eastern slope was intensely settled and this sector was
the center of large-scale pottery production. The excavation
has enabled us to identify ten well-preserved overlapping lay-
ers close to the surface (figs. 11-12) and almost the whole
sequence has shown traces of pottery production or firing
structures. These are remarkable for their quantity, technical
features, concentration and permanency in a same area during
a time span of several generations.
Although it is likely that during the first half of the 4th mil-
lennium BC Girdi Qala was an indigenous Late Chalcolithic
settlement (with a southern enclave probably located on the
north mound), the large majority of the ceramic assemblage
collected in Trench C belongs to South Meso potamian (Uruk)
classical traditions. This is why this sector provides unex-
pected information about the organization of the productive
systems, as well as new evidence for relations between local
inhabitants and South Mesopotamian settlers.
The stratigraphic sequence, with many phases concen-
trated in a relatively short period, testifies to the intensity of the
production, which implied frequent refurbishment and recon-
structions of the firing structures:
– Level 10 has yielded five huge two-storey pottery kilns
(2053, 2055, 2056, 2057 and 2060; fig. 13) connected to
each other by a ventilation duct. Their average dimen-
sions (above all concerning 2053 and 2055), with diam-
eters ca 1.8 m, are quite exceptional for the Chalcolithic
Fig. 10 – Overview of the 4th millennium ramp near Trench B, from the east.
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70 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
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period (Hansen Streily 2000: 80). The heating chambers
are uniform in depth and the aeration channels were at
the same height, indicating that all the features were
designed as a single complex;
– Level 9 is represented by two large perpendicular walls
(2058, which cuts kiln 2060 of the bottom level, and
2059), made of bulky stones and three rows of mud
bricks above the stones. The size and the careful con-
struction of these walls suggest that they probably bor-
dered buildings of some importance;
– Level 8 is composed of two round pottery kilns (2051
[fig. 14] and 2052). Unlike the kilns identified in the
deepest level, they were independent installations. The
firing chamber of 2051 has been completely excavated,
while that of 2052 has been partially emptied and an
interior section has shown different filling layers and
several layers of clay applied on the interior walls. It
clearly indicates an intensive and long-lasting activity.
A bench (2061, with one row of bricks conserved on five
layers of bricks) was connected to the kiln 2052. An out-
door floor (2054), facing the two installations and prob-
ably used for drying pots, was also identified;
– Level 7 is composed of several firing installations. The
main complex of kilns is represented by three circular
structures (2035, 2036, 2037; figs. 15-16) connected
by an internal ventilation shaft and by an external duct
devoted to evacuate the smoke (by a chimney [2049]
looking like a small cell on the eastern side of the trench,
delimited by walls 2046 and 2048). These three instal-
lations are similar in shape and size: the eastern one
(2037) was excavated by taking out a section of the fir-
ing chamber and pierced sole, while the two other firing
chambers were emptied, yielding a great deal of slag and
firing waste. Three other kilns, 2032, 2033 and 2034, in
the northern sector of the exposed surface, were sepa-
rated and independent structures, but their basic firing
system was the same, that is an up-draught two-storey
system. The small kiln 2032, only partially preserved
and cut by the structures of Level 6, had a sub-circular
mouth to supply the fuel on the southern side. Even if
kilns 2034, 2032 and 2033 were built a little higher up
on the slope, they were contemporary with the triple kiln
(2035-2036-2037) because they were associated with
the same external floor. As in Level 10, the complex fir-
Fig. 11 – Girdi Qala. Trench C, general view from the southwest.
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 71
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ing structure is composed of several kilns connected by
a duct is absolutely unique in the technical panorama of
ancient Mesopotamia;
– Level 6 is composed of two rectangular units (2028 and
2029) and maybe a third structure on the western side.
These small rooms were enclosed by walls 2030, 2044,
2043, 2042, 2041, 2048, 2039, 2038 and 2027. This
locker or pigeonhole structure could be interpreted as a
granary, but also as basins for clay decantation because
of the lime coating on the internal surface of its walls.
This is an important point to clarify during future cam-
paigns. In fact, if this structure was a warehouse, then this would
mean that the stratigraphy shows an interruption of the use of
this space as an area for firing pottery (a food store would never
Fig. 12 – Girdi Qala, plan of Trench C.
2058
2059
2060
2057
2055
2056
2061
5000
2006
2007
2013
2026
2010
2004
20122015
2001
2003
2005
2008
2009
2017
20162018
2021
2045
2019
2020
2027
20252030
20322034
2033
2028
2029
20442043
2037
2040
2039
2038
2041
2042
2035
2036
2050
2046
2048
2049
2053 2052
2051
N
0 5 m
Girdi Qala 2015Plan of Trench C
Level 1Level 2Level 3Level 4Level 5
Level 6Level 7Level 8Level 9Level 10
7-1 : Early LC 310-8: Late LC 2
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72 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
have been built next to the kilns because of the danger of fire;
Moorey 1994: 154). Otherwise, if this pigeonhole structure was
a basin for refining clay, the kilns would not be the only craft
structures concentrated in one area, but large workshops would
have been built at the edge of the village, something which
would imply a different organization of the production system;
– Level 5 is represented by the walls 2019 and 2020,
delimiting a room (2025);
– Level 4 comprises the walls 2016, 2017 and 2026. These
delineate a large room, where an indoor floor has been
brought to light (2018). Another wall (2021), delimiting
another room (2045), has been identified on the western
side of the trench: it is parallel to 2017 and perpendicular
to 2016;
– Level 3 is composed of two perpendicular walls (2000
and 2013). Even if the walls have been identified on the
bottom of Level 2, their massive structure is three-rows
of bricks wide.7 An outdoor floor (2022) was associated
with this level;
– Level 2 is composed of the walls 2004, 2006, 2007,
2008 and 2010. They delineate a small rectangular fully
excavated unit (2005) and two other units in the north-
western sector of the trench. Further excavations are
needed to establish if this building could be interpreted
as a tripartite dwelling.
Indeed, for the Levels 6-2 the same question—whether the
constructions brought to light belong to dwellings and ware-
7. The average dimensions of the bricks are 55 x 35 x 15 cm in Levels 10-8
and 40 x 25 x 15 cm in Levels 7-2.
houses or rather to large ceramic workshops centralizing struc-
tures other than kilns—will have to be resolved during future
campaigns. In particular, the walls of Level 2 seem to delin-
eate a tripartite (perhaps domestic) edifice and, in this case,
there would be no continuity in the use of the southern slope
for craft purposes. But, at the same time, during the first half
of the 4th millennium BC a partitioned structure and large
walls do not always indicate a house, as demonstrated by the
workshops at Tell Brak TW20-TW19, Grai Resh IIB or Tepe
Gawra X spaces 1085-1086 and annexes (Oates et al. 2007;
Kepinski 2011: 37, fig. 13; Rothman 2002: fig. 3.10);
– Level 1 is represented by three kilns (2012, 2015 and
2001). These installations have cut the walls of the pre-
vious Level 2. A floor associated with these kilns is vis-
ible in the northern section of the trench.
FIRING TECHNOLOGIES
Apart from some structures interpreted as domestic units
or utilitarian buildings, the main results from Trench C are
definitely the working spaces and firing installations. Some
comparable contexts from other Uruk sites have never been
extensively published, such as the firing area from Tell Qraya,
on the Middle Euphrates, with over 40 kilns and fire installa-
tions (Reimer 1989). In the same way, other craft areas for
ceramic production are difficult to interpret, such as the kilns
in the courtyard of NC-NF compounds at Djebel Aruda (van
Driel and van Driel-Murray 1983: 22-23, Map 3). Trench C at
Girdi Qala offers limited evidence for the firing area, although
Fig. 13 – Girdi Qala. Trench C, view of the kilns of Level 10 (2053, 2055, 2056, 2057, 2060) and Level 8 (2051 and 2052), from the north.
Fig. 14 – View of the kiln 2051 (Level 8) from the south.
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 73
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for the moment it is not possible to understand its internal
organization. However, several firing installations have been
identified and some of them are absolutely remarkable. All the
kilns have yielded Southern Uruk ceramics (from the filling
layers, accumulated when the installations were already dis-
used, but also from the bottom of the firing chambers, which is
an in situ context). Local Late Chalcolithic finds come exclu-
sively from walls and filling layers accumulated on the floors
and between the different levels. This indicates that South
Mesopotamian craftspeople were the only firers of ceramics in
the large area on the slope of Girdi Qala.
From a technological point of view, the firing installations
belong to a well-known two-storey up-draught type of pottery
kilns. These kilns appear in the Halaf-Ubaid phase and spread
in the 4th millennium throughout the Uruk cultural area in
Fig. 15 – Girdi Qala Trench C. Triple kiln of Level 7 (2037-2035-2036), view from the west.
Fig. 16 – Girdi Qala Trench C. Plan and section of triple kiln of Level 7.
20322034
20332037
2035
2036
2050
2046
2048
2049
N
0 1 2 m
A
A’Girdi Qala Trench C: Level 7
2037 2035 2036
A A’
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74 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
Mesopotamia (in the south as well as in the north) and Western
Iran (Delcroix et Huot 1972; Majidzadeh 1977; Hansen Streily
2000). Some samples of these kilns used for firing Southern
Uruk ceramics are known from Choga Mish Protoliterate
period, Tell Rubeidheh, Tell Ahmad al-Hattu, Kirbet Hatara or
Abu Salabikh.8 But the multiple kilns of Girdi Qala Trench C,
in Levels 10 and 7, had never been documented so far.
These complex kilns, composed of many furnaces con-
nected to each other, have yielded exclusively ceramics belong-
ing to the South Mesopotamian tradition and therefore
constitute a hitherto unknown Uruk firing technology. Even if
consisting in several up-draught kilns, these firing structures
cannot be considered as the mere result of the juxtaposition of
separated furnaces of a previously well-known type. From an
architectural point of view, the multi-kiln complexes of Levels
10 and 7 have been conceived as unitary structures (fig. 16). As
demonstrated by the uniform height of the ventilation chan-
nels, as well as by the structural connections and entangle-
ments between some of the heating chambers (such as
2035-2037 in Level 7 and 2055-2056-2057-2060 in Level 10),
these facilities were built as unitary large installations. For
2035-2037 and 2055-2056-2057-2060, this means that each
circular chamber was not built independently from the other(s):
each includes bricks which also belong to the adjacent firing
space. This indicates that the construction was not carried out
as for a series of distinct kilns (one chamber after another), but
rather by building all the chambers at the same time, a row of
bricks after another. This method was also quite flexible, since
it enabled other chambers to be added by digging a nearby pit,
lining it with bricks and connecting it to the other chambers
through a ventilation duct (at the same level as the other heat-
ing spaces). It is the case of the heating chamber 2036, which
is part of the triple kiln 2035-2036-2037, but without being
structurally linked to 2035-2037. In fact, 2036 has been added
and connected to a previous double kiln (constituted by 2035-
2037). This is not just further evidence for a frequent and
intensive production. This kind of firing installation shows that
the Ubaid and post-Ubaid up-draught technology was not only
perfectly mastered (Kingery 1997; Pool 2000),9 but also sig-
8. See Delougaz and Kantor (1996: 29, pl. 275); Alizadeh (1983: 39); Nöldeke
(1937: 7); Delcroix et Huot (1972 : 66); Killick et al. (1988: 18); Sürenhagen
(1979: 48); Fiorina (1997: Figs. 12, 13 a-c); Postgate and Moon (1982: 127).
On the other hand, during the Late Chalcolithic, circular up-draught two-
storey kilns are not a specificity of the Southern Uruk, but rather a long-
standing Ubaid tradition, in the South as in the North (as demonstrated by
the LC2 kilns of Tell Musharifa; Numoto 1987: Fig. 12). The Late Uruk/
Proto Ninevite 5 kiln of Tell Karrana 3 shows the continuity of the same
technology after the Uruk phase (Wilhelm and Zaccagnini 1993: Fig. 16).
9. The same up-draught technology was also used in a large Late Uruk rect-
nificantly improved by the craftsmen. In fact, the same modu-
lar criterion observed for the architecture of the kilns is also
applied to the cycles of firing on the technological level. Even
if it would have been possible to place vessels in one single fir-
ing chamber (the upper one), the presence of ventilation ducts
between the heating chambers (the lower ones) implies that,
once one of them had been used (with the fuel burning inside),
all of them would be heated. Despite the limited size of the
duct, it is sufficient to establish a partially horizontal circula-
tion of the heat (Gosselain 2002: 161), even if the main draft
remains vertical. In other words, the multi-kiln structures were
built as unitary constructions because designed to operate as
unitary devices.
In terms of their structural and dimensional features, these
are remarkable installations. They also provide unsuspected
evidence for mastery of very complex technology in the Early
Uruk phase.
THE CERAMIC ASSEMBLAGE OF GIRDI QALA AND LOGARDAN
In the light of this unexpected evidence for pottery kilns,
the ceramic assemblage has been studied not only to establish
a consistent relative chronology, but also as a means to investi-
gate the production systems. The chronological issue is funda-
mental because the Chalcolithic phases in the western Qara
Dagh region (and, more generally, in the northern sector of
Central Mesopotamia) have never previously been studied. On
the other hand, the presence of a large amount of South
Mesopotamian Uruk sherds has provided an opportunity to
observe the modalities of the diffusion of the Uruk material
culture in this area, as well as its interaction with the local pot-
tery traditions. This is the central topic of all the archaeologi-
cal literature about ‘culture contact’: to recognize and
understand culturally-particular ways of envisioning and rep-
resenting the ‘own’ and the ‘foreign’. The implicit assumption
in the archaeological approaches to the ‘Uruk expansion’ is
that there are two distinct cultural entities represented by two
different material cultural assemblages: the ‘Uruk’ and the
‘local’. From a ceramic point of view, the easy distinction
between an indigenous traditional chaff-faced tempered
ceramic assemblage (Marro 2010) and a mineral tempered
angular bitumen (or brick) furnace at Uruk (Nöldeke 1937: Plan 27.b).
Despite the functional difference, it confirms a use of the up-draught
installations for large-scale productions.
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 75
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South Mesopotamian tradition (Wright 2014) is a schematic
analytical tool. It enables us to establish a classificatory dichot-
omy between sites affected by an ‘Uruk’ presence (such as
Hacınebi, Nineveh, Tell Brak: Pollock and Coursey 1995 and
1996; Pearce 2000; Gut 1995 and 2002; Oates and Oates 1993)
or just involved in the exchange network (like Zeytinli Bahçe,
Leilan, Kenan Tepe or Tell Feres: Balossi Restelli 2006;
Schwartz 1988; Creekmore 2007; Forest et al. 2012; Vallet
2014 and in press). However, there are potential problems with
this kind of schematic division of the cultural panorama into
two distinct groups. First, the ‘local’ and the ‘Uruk’ taxono-
mies create internally undifferentiated entities represented by
ideal artifact types. Secondly, they are analytic categories cre-
ating arbitrary and static cultural boundaries, while the rela-
tionships between ‘Uruk’ and ‘local’ cultural traits and people
changed over time.10
These problems are even more serious in a region like the
Qara Dagh area, where almost nothing is known about the
Uruk expansion. Indeed, the whole north-eastern side of the
Mesopotamian alluvium is quite poorly known. Some data are
available for an Uruk presence in Nineveh (Gut 1995) and in
the Hamrin (Killick et al. 1988; Sürenhagen 1979). But, since
many decades, the concentration of archaeological research in
Syria has created the (false) impression that the Euphrates was
the main (and almost the sole) route of the Uruk expansion.
The Qara Dagh appears as a major area for the understanding
of when and how Uruk people settled in Central and Northern
Mesopotamia.
In order to reconstruct some cultural dynamics underlying
the production processes, the sherds (5627 from Girdi Qala
and 64 from Logardan:11 rim, bases and decorated sherds as
well as common body fragments) have been examined to rec-
ognize traditional chaînes opératoires.
METHODOLOGICAL PROCEDURE
In the technical analysis of the ceramic materials from Girdi
Qala and Logardan, all aspects of the ceramic chaînes opéra-toires have been examined in order to encompass all stages of
the manufacturing process, traditionally disregarded to analyse
just shapes and decorations, seen as the only vectors of differ-
ences between “cultures” – “derniers degrés de fait” according
10. More generally, the essentialist approach to the “Uruk” and the “local”
implies all the problems intrinsic to the notion of “archaeological culture”
(Welsch and Terrell 1998; Veit 1994; Baldi 2013b: 17-18).
11. 4987 sherds were collected at Logardan, but only 64 of them date back to
the 4th millennium and are consistent with the topic of this paper.
to Leroi Gourhan (1945: 30). The classificatory analysis of the
sherds highlights different technical traditions corresponding to
different producer groups, according to a methodology already
employed for Chalcolithic assemblages from the Levant (Roux
and Courty 2005 and 2007; Baldi 2013b) and Northern
Mesopotamia (Baldi 2012a, b and c; 2013a). Shaping methods,
surface treatments, petrographic compositions of the pastes, fir-
ing procedures and morphological variants of the assemblage
have been sorted so as to identify traditional ways to produce
ceramics, specific to certain social groups.
As demonstrated by recent ethno-archaeological and
anthropological studies about technical behavior and social
boundaries (Gelbert 2003; Gosselain 2002; Patton 2008; Stark
1998; Stark et al. 2008), each chaîne opératoire is typical of a
particular group of craftspeople because it was transmitted
through generations by a specific network of apprenticeship
(Wallaert 2001 and 2008; Gosselain 2008). Therefore, it
expressed the technical identity of the social group underlying
the technical tradition (Roux and Courty 2005 and 2007; Roux
2010; Baldi 2013a and b). Hence, the different traditional
chaînes opératoires can be observed in their synchronic spa-
tial distribution as well as in their diachronic evolution through
conservatism, borrowings (i.e., in their continuities), disap-
pearance of some of them and emergence of some innovations
(that is in their discontinuities).
The first part of the study involves distinguishing technical
entities and their variants: recurrent combinations of macro-
traces of fashioning and finishing show a set of specific opera-
tions or techniques that correspond to different technical
groups. In a second phase, within the different technical
groups, all sherds are classified to sort their petrographic
features, both on the basis of the fine mass (its colour, aspect
and granulometry) and of non-plastic inclusions (nature, size,
distribution, morphology and quantity). The third and conclud-
ing stage of the analysis is represented by the morphological
and stylistic classification (as in traditional typology) of the
sherds within each techno-petrographic group (Roux 2010).
TECHNICAL FEATURES OF THE CERAMIC PRODUCTION
At Girdi Qala, Levels 10-1, vessels (fig. 17) were shaped by:
1) a moulding technique;
2) overlapping coils (namely rings) of 2-2.5 cm thick;
– 2.i) wheel-coiling technique by overlapping coils of
2 cm thick and finishing the containers by the rota-
tional kinetic energy;
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76 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
3) overlapping flattened coils of 3-3.5 cm thick;
– 3.i) wheel-coiling technique by overlapping coils of
3.5 cm thick and finishing the containers by the rota-
tional kinetic energy.
The autoptic analysis of the macro-traces depending on the
different shaping techniques clearly indicates that wheel-coil-
ing, attested by some rare and fine small-sized bowls, consti-
tutes a complex and uncommon variant of two distinct coiling
traditions (2 and 3). These ones are characterized by an impor-
tant dimensional difference of the coils and by an unlike dis-
position of the junctions (sub-elliptic section with external
oblique orientation for the Technique 2 vs sub-elliptic section
with alternating oblique orientation for the Technique 3).
The restricted number of techniques and petrographic vari-
ants indicates that, as already demonstrated for other areas of
the 4th millennium in Northern Mesopotamia (Baldi 2012c and
d), the ceramic production was a very hierarchized and cen-
tralized activity, conducted by a restricted number of special-
ists. These artisans were in charge of the manufacture for large
groups, exceeding by far the horizon of their own village com-
munity. Future campaigns will clarify this panorama, but so
far it does seem to fit the evidence from the kilns in the central-
ized firing area at Girdi Qala Trench C.
Four main petrographic macro-groups have been identified
(fig. 17):
1) Group A: beige or light orange porous fabrics, fired in an
incomplete oxidizing atmosphere during short firing
cycles (grey or black core), with abundant coarse vegetal
and dispersed mineral inclusions (mainly basalt, quartz,
sub-angular calcite, ferruginous particles and micas);
2) Group B: beige and light orange dense mineral fabrics,
fired in oxidizing atmosphere, with traces of serpentine
and carbonates in the fine mass of the clay, and signifi-
cant quantities of grinded shells and ferruginous
inclusions;
3) Group C: orange-reddish fabrics, fired in incomplete
oxidizing atmosphere (short firings, black core) with
large vegetal and small-sized mineral inclusions (basalt,
limestone) and coal particles;
4) Group D: orange-brownish fabrics, fired in reducing
atmosphere (grey core and surfaces), with abundant
basalt, quartz and metamorphic inclusions (silicates,
chlorite, marble, etc.).
Petrographic Groups A and B gather different common
wares and some (rare) fine wares (with depurated small-sized
inclusions), while Groups C and D match with cooking wares.
On the one hand, fabrics belonging to Groups A and C per-
fectly fit the definition of the well-known North Mesopotamian
Late Chalcolithic ‘Chaff-Faced’ wares. Indeed, they represent
the local version (with raw materials readily available in the
Qara Dagh) of the large North Mesopotamian ‘Chaff-Faced
koiné’ (extended from Central Mesopotamia to the Southern
Caucasus: Marro 2010). On the other hand, the Groups B and
D reflect the South Mesopotamian mineral tradition (Helwing
2002). This general framework includes some (rare) specimens
belonging to Groups A and B sharing firing in a reducing
atmosphere and, therefore, a grey aspect. These grey wares can
be coarse chaff-faced vegetal (A) or mineral and relatively fine
(B) tempered wares.
This quite sharp division is also apparent on the basis of the
shaping methods, since techniques 2-2i and 3-3i are always
respectively associated with local (A-C) and southern (B-D)
fabrics.12 These technical traits seem to confirm a sharp divide
between the ‘Uruk’ and the ‘local’. But the technical panorama
is not really dichotomous. Indeed, even if the shaping by
moulding represents a minority of the vessels (about 16%), it is
indistinctively associated with both North and South
Mesopotamian wares. Besides, it is often associated to culi-
nary vessels in C or D pastes. Further studies (and a longer
chrono-stratigraphic sequence) are needed to establish whether
Technique 1 constitutes a remnant of an ancient shaping
method that gradually disappeared in the LC3, or rather an
innovation that has spread (and in this case, was it a North or
South Mesopotamian native innovation?).
MORPHO-STYLISTIC FEATURES: REGIONAL PARALLELS AND RELATIVE CHRONOLOGY
The ceramic assemblage of the Trench C Levels 10-1 at
Girdi Qala and Trenches A, B and C Level 4 at Logardan can
be generally ascribed to the local LC2-LC3 (South Meso -
potamian Early Uruk phase). It means that the ten levels recog-
nized on the southern slope at Girdi Qala correspond to a
relatively short time span.
Nevertheless, a difference is quite evident between
Levels 7-1, dating back to the beginning of the LC3 North
Mesopotamian horizon, and Levels 10-8, whose ceramic
assemblage belongs to the late LC2 North Mesopotamian rep-
ertory. The whole sequence yielded a large amount of Southern
Uruk pottery, representing a clear majority (ca 69%) of the 915
diagnostic sherds. Therefore, the chronology can be defined
12. Obviously, rare and fine wheel-coiled 2i and 3i little bowls are respec-
tively associated with fabrics A and B, and never with culinary coarse
fabrics of the Groups C and D.
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 77
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0
5 cm
SH
AP
ING
TE
CH
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SFA
BR
ICS
0
5 cm
A B C D
0
1
Common wares Cooking wares
“Uruk” wares
“Local” wares
2 2.1 3 3.1
Fig. 17 – Schematic representation of the chaînes opératoires (on the basis of their main phases) within the 4th millennium ceramic assemblage of Girdi Qala.
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78 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
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using the terminology generally adopted for Southern
Mesopotamia: it covers the end of the Early Uruk phase and
the very beginning of the Middle Uruk period. In other words,
it seems that this sequence documents the oldest Uruk pres-
ence known in Central and Northern Mesopotamia.
However, the morpho-stylistic analyses confirm the pres-
ence of two distinct traditions: the indigenous one, character-
ized by North Mesopotamian shapes and chaff-faced fabrics
(Groups A and C) and the South Mesopotamian one, with min-
eral pastes (Groups B and D) and Uruk-related shapes.
Levels 10-8 show a local repertory of the beginning of the
4th millennium (late LC2), already devoid of Ubaid-related tra-
ditions. Indeed, there is no trace of fine thin-walled beakers,
everted rim urns and serially produced Coba bowls with
scraped rounded bottoms.13 In the same way, painted decora-
tions are totally absent. Some V-shaped Wide Flower Pots with
flattened bases are attested, but they are no longer ‘mass’-pro-
duced (as in the previous LC1 and early LC2 phases in Gawra
XII-XI, Nineveh, Khirbet Hatara or Tell Brak CH13).14 In the
late LC2 assemblage, one can recognize the outcome of the
converging processes of regionalization and homogenization
that had occurred over centuries in Northern Mesopotamia.
On the one hand, the assemblage of Girdi Qala shows specific
micro-features, which appear different from the Gawra-
Nineveh area and from the Zammar region. In particular,
flaring-rim jars have thinned and pinched rims (fig. 18: 1) and
samples of beaded rims15 are very rare; cannon spouts are spo-
radic and have flared trumpet-like edges (fig. 18: 2),16 while
double rim jars and neckless jars with sharply everted rims
(flange-rim jars) have relatively short rims (fig. 18: 3-4 and 7)
compared with the samples from Gawra X-IX or Hamoukar
‘southern extension’.17 On the contrary, very close parallels can
be identified for all these shapes with Yorghan Tepe.18 Anyway,
similar local particularities are well documented in every
meso-region of Late Chalcolithic Northern Mesopotamia
(Helwing 2000; Baldi and Abu Jayyab 2012). On the other
hand, the ceramic repertoire appears very homogeneous, when
compared to the North Mesopotamian general typology. Hole-
13. But some specimens of Coba bowls have been collected on the surface,
which suggests the presence of LC1 in situ levels in the deepest strata.
14. See Rothman 2002: Pl. 14.1460; Gut 1995: Pl. 53.795-798; Fiorina 2001:
Figs. 2.3-4, 3.15-23; Oates 1987: Fig. 3.4-5.
15. For flaring-rim jars with a beaded rim see Abu Jayyab 2012: Fig. 9.5.
16. At Tepe Gawra, an isolated specimen, quite different from the other local
common spouts, is similar to the samples from Girdi Qala (see Rothman
2002: Pl. 12.1453).
17. See for instance the specimens with quite developed rims in Rothman
2002: Pl. 20.2245; Abu Jayyab 2012: Fig. 13.6-8.
18. See Starr 1937: Pl. 42.
3
4
1 2
6
5
7
0 5 cm
Fig. 18 – Ceramic types from Girdi Qala Trench C. Late LC2 jars.
mouth, flange-rim and double mouth jars are well documented
at Girdi Qala Trench C 10-8, as well as inward bevelled-rim
bowls (fig. 19: 1-2), cannon spouts, little-sized fine carinated
bowls (fig. 16: 5-6) and a small quantity of fine wheel-coiled
bowls (fig. 19: 3-4). The same assemblage is documented in
Tell Brak, Nor untepe, Gawra, Grai Resh, Yorghan Tepe,
Qalinj Agha, Khirbet Hatara, and Musharifa.19
According to Gut (1995: 256-258) and Rothman (2002: 56)
terminology, the late LC2 assemblage from Girdi Qala
Trench C 10-8 clearly belongs to the so-called ‘Gawra B’ phase
(like at Gawra X-VIII, Hammam et-Turkman late VB, and Tell
Brak TW 21-20), characterized by a rising proportion of bowls
with inward bevelled rim and thick flattened rim.20 Since this
LC2 period, the majority of the indigenous assemblage is
19. See Oates 1986 and 1987; Oates and Oates 1993; Hauptmann 1972; 1976;
1979 and 1982; Gut 1995: 248; Starr 1937-39; Lloyd 1938 and 1940;
Numoto 1987: Fig. 14.
20. The so-called “Gawra A” phase (documented at Gawra XIA-XA,
Hammam terminal VA – early VB, Hamoukar phases 3-1), characterized
by the last samples of thin-walled beakers, post-Ubaid painted wares and
Coba bowls, has not yet been reached.
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 79
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represented by morphological categories which continue in the
LC3 phase: hole-mouth types (fig. 18: 6), “S”-shaped rim jars
(fig. 18: 5), bowls with inwards bevelled rim and club-headed
bowls (fig. 19: 7-8). In the whole of Northern Mesopotamia, the
latter type announces the appearance of the ‘hammerhead’
type, as in Hacınebi A and Brak HS1.21 Its presence in the Qara
Dagh area is remarkable because, as in the whole sector east of
the Tigris River (Gavagnin et al. 2016),22 real Hammerhead
bowls are virtually absent during the LC3.
Indeed, between late LC2 and early LC3, the assemblage of
Girdi Qala shows a remarkable morpho-stylistic continuity, as
well as including some diagnostic shapes of the transitional
phase (hole-mouth with beaded or triangular-section rims,
short neck jars with internal angled rim, club-headed bowls,
fine carinated bowls and grey carinated bowls with everted
rim). These transitional types have close parallels at Tell Feres
4b-4a, Tell Brak TW 20-19, Hamoukar ‘southern extension’
Level 1, Hammam et-Turkman late VB and Tell Boueid II.23
In the first part of LC3, all these types are still attested. In
particular, despite the absence of genuine hammerhead bowls,
the club-headed type is always moulded according to the
Technique 1. The morphology of these bowls is close to the
early type of hammerhead containers, with an in-turned rim
(or thickened on the interior side; fig. 19: 7-9) like in Brak HS1,
Leilan V, Hacınebi A, Nineveh -45-37 ‘Norduruk A’.24 Their
late morphology, with a rim thickened on both the interior and
exterior side,25 is documented by only one example from the
surface collection.26 In the same way, the other main hallmark
of the North Mesopotamian LC3-LC4 assemblages, i.e. cari-
nated casseroles, is also virtually absent.27 Moreover, it is
remarkable that coarse conical bowls with a pouring lip (Boese
1995: 84, fig. 21) are not documented at all. On the contrary,
some internally hollowed-rim28 or angled-rim jars29 are attested
21. See Pearce 2000; Matthews 2003: Fig. 4.17:12.
22. The same absence of hammerhead bowls is documented on the other side
of the Qara Dagh mountains, at the site of Kani Shaie in the Bazian Valley
(A. Tomé and S. Renette, personal comm.).
23. Baldi and Abu Jayyab 2012: Fig. 6; Akkermans (1988: Figs. 107.97,
108.107); Suleiman and Nieuwenhuyse (2002: Fig. 8.1.17).
24. See Matthews 2003: Fig. 4.17.12; Schwartz 1988: Fig. 57.2; Pearce 2000:
Figs. 5.a-e, 6.c; Gut 1995: Pl. 58.853-857.
25. Rova 1999-2000: Fig. 5.2.
26. The dating of this much eroded specimen to the LC3-4 is hypothetical.
27. This feature is also shared by a wide area east to the Tigris river, as dem-
onstrated by the LoNAP survey (Gavagnin et al. 2016) and by the French
Archaeological survey of the Sulaymaniyah Governorate in the area of
the Rania plain (directed by J. Giraud).
28. See for instance LC3 samples from Tell Brak CH9-12 (Oates 1985:
Figs. 1.13, 2.17-18), Hacınebi (Pollock and Coursey 1995: Fig. 8.J; Pearce
2000: Fig. 4e-g) and Leilan V (Schwartz 1988: Fig. 60.5).
29. See for instance LC3 samples from Kenan Tepe 6-7 (Creekmore 2007:
12
3 4
56
7
8
10
11
12 13
9
0 5 cm
Fig. 19 – Ceramic types from Girdi Qala Trench C. 1-9) Local late LC2 – early LC3 bowls; 10-13) Southern Uruk bevelled-rim bowls from late LC2 and early LC3 contexts.
(fig. 20: 1-3) and, according to a quite early dating, have a more
developed neck than that of the late LC3 and LC4 specimens.30
Therefore, even exclusively on the basis of the indigenous
ceramic materials, it is evident that Levels 7-1 of Girdi Qala
Trench C date back to the early LC3 and do not show any trace
of late LC3 and LC4 diagnostic types.
But during the whole sequence local shapes in chaff-faced
wares represent a minority (31%) of the assemblage. The large
majority of the ceramics are of Southern Uruk morphological
Fig. 11.A, J), Zeytinli Bahçe (Balossi Restelli 2006: Figs. 9.G, 11B-C, H,
K, and 12.A-F) and Tell Brak CH9-12 (Oates 1985: Fig. 1.13).
30. For samples of LC4 hollowed-rim or angled-rim jars with short neck, see
Rova 2007: Group 4 – O.3, O.5.
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80 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
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tradition and their typology is consistent with an Early Uruk
(Eanna XII-IX) chronology (Wright 2014). As well as bevelled-
rim bowls (or rather proto-bevelled rim bowls, with the rim
sometimes slightly rounded and never sharply bevelled),
Levels 10-8 have yielded some jars with inaccurate and crude
(i.e., the earliest variety) cross-hatched decorations,31 rare bands
of impressed dots, shallow basins (fig. 20: 4, 7-10), short necked
jars with upwards spouts and sharp angled-rim jars. Starting
from Level 7, these southern types become more frequent and
differentiated, with flaring or rectangular rim spouted jars, verti-
cal pierced handles (fig. 20: 5-6) and sharp angled jars with tri-
angular rim. All these shapes are always attested with their early
morphological features (for instance, spouts are quite short—
like examples from Sheikh Hassan 13-10, Nineveh ‘Norduruk A’
or Susa 22-21—and never drooping and downwards curved)
(Bachmann 1998a; Gut 1995; Le Brun 1971 and 1978a and b).
Since the late LC2, the most frequent Uruk type is repre-
sented by bowls with bevelled rim (fig. 19: 10-13), first charac-
terized by a loosely oblique rim, then, at the beginning of the
LC3, by the mature shape. This widespread South Meso-
potamian material is remarkable because, despite many old-
dating misconceptions, they are not serially produced at all.
On the contrary, they show many technical and morphological
differences (they are shaped by Techniques 1, 2 and 3, with
rims sometimes thinned, rounded, or cut and bevelled in vari-
ous ways and with varying orientations). Moreover, although
they are considered as the main indicators of the Southern
Uruk ceramic assemblage, their pastes belong both to A (chaff-
faced, supposed to be ‘local’) and B (mineral-tempered, sup-
posed to be ‘Uruk’) petrographic groups. All these features
seem to describe material whose production did not respect the
separation between local and southern traditions. Further stud-
ies are needed to establish the reasons for the unexpectedly
hybrid character of these bowls that are generally considered
as the hallmark of Southern Uruk. But one can speculate that
this blending of technical traditions could indicate very early
technical borrowing (as attested during the LC4-5 in Hassek
Höyük, Tell Feres and Zeytinli Bahçe).32 Such a cultural inter-
penetration would be consistent with very early and stable rela-
tions between local and southern people.
Starting from Level 7 (beginning of the LC3), mineral-tem-
pered Southern Uruk types increase in number. Sharply everted
rim jars, bevelled-rim bowls (with more regularly bevelled
31. See for instance at Nineveh MM.-37-21 (Gut 1995: Pl. 59-68) and Tell
Sheikh Hassan (Bachmann 1998a: Figs. 8.b, d; 10.c-d; 12-13).
32. See Helwing 2000 and 2002. Concerning Zeytinli Bahçe, M. Frangipane,
personal comm.
1
2
3
4
7
8 9 10
5 6
0 5 cm
Fig. 20 – Ceramic types from Girdi Qala Trench C. 1-3) Early LC3 jar; 4-10) Early Uruk – Middle Uruk southern types from late LC2 and early LC3 contexts.
rims) and jars with incised shoulders are more frequent.
Incisions (crosshatched bands and triangles, horizontal lines,
impressed ribs and punctuations) are more regular (fig. 20: 8-9),
while the average dimensions of the storage jars increase sig-
nificantly. The ceramic material from the stone ramp
(Trenches A and B) at Logardan perfectly matches the assem-
blage from Levels 7-1 of Trench C at Girdi Qala.
CONCLUSION
If analysed separately, the indigenous and Southern Uruk
assemblages do not portray any unusual features. But they are
not separate repertoires: they are a single assemblage and, in
this sense, it is anomalous to find associated in the same strati-
fied contexts (as far as Levels 10-8 of Trench C at Girdi Qala)
both indigenous late LC2 shapes and southern Early Uruk
diagnostic types. Chronology is not a problematic issue in
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New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 81
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
itself, because local late LC2-early LC3 ceramics and Early
Uruk-Early Middle Uruk potteries are contemporaneous. What
is surprising is their coexistence and concomitance in the same
site during a very early period.
Despite longstanding assumptions that the Uruk expansion
started during the late LC3 phase (or southern ‘Middle-Uruk’
phase: Rothman 2002; Stein 2001; Helwing 2002; Rothman
and Badler 2011; Gopnik and Rothman 2011; Gut 2002), it is
now clear in the Qara Dagh area that contact with Southern
Uruk people occurred from a very early period (late LC2). In
terms of absolute chronology, the Uruk expansion at Girdi
Qala does not appear ca 3600 BC (the date supposed for the
entire North), but rather ca 3900 BC.33 Incidentally, the Qara
Dagh seems to represent the limit of this expansion in the late
LC2, as there is not (yet) evidence of a Southern Uruk manifes-
tation east of this range before the LC3.
Furthermore, in Trench C at Girdi Qala, Southern Uruk
materials not only make up the majority of the assemblage but
they are also the only ones from in situ contexts. All the mor-
phologically indigenous sherds in chaff-faced fabrics (A and
D Groups) come from filling layers, walls or open-air work-
spaces. This indicates that all the furnaces and firing installa-
tions were used to fire Uruk ceramics. In other words, South
33. Such a dating is paralleled by another noticeable evidence, provided by
the presence of well-stratified Uruk materials in late LC2 levels at Grai
Resh, in the Sinjar area (Kepinski 2011: 37). However, Grei Resh yielded
no trace of Southern Uruk ceramic production or presence of southern
people during the late LC2.
Mesopotamian people had a centralized workspace for their
own activities that was not shared with local artisans. On the
other hand, despite the relatively short time-span covered by
the excavated sequence (between late LC2 and early LC3),
many technological features reveal borrowing and hybridiza-
tion from a very early phase.
This kind of organization and spatial pattern, with a very
early foreign presence, segregated spaces and ceramic traditions
in close contact, opens the way for future research on the chro-
nology (table 1) and collaborative processes involved in Uruk
culture expansion in Central Mesopotamia. In particular, the
fundamental dichotomy which still shapes the approach to the
Uruk expansion had been nuanced to reassess the essentialist
nature of notions such as North vs South, or ‘core’ vs ‘peri phery’.
But the spatial and technical modalities of the encounter between
these two traditions have never been the focus of the analysis.
On the contrary, the evidence from Girdi Qala and Logardan
suggests that it will soon be possible to observe how local and
foreign traditions intertwined, as well as their distribution within
residential and architectural spaces. As for Uruk ceramics,
whose local production at Girdi Qala confirms recent studies on
other Uruk assemblages in Northern Mesopotamia (Emberling
and Minc 2016; Minc and Emberling 2016),34 the analytical
34. Indeed, it has to be emphasized that our discoveries mirror the results of
the Uruk pottery analyses by G. Emberling and L. Minc, showing that
there was virtually no (long-distance) trade in ceramic vessels in the Uruk
network. But despite this we would not conclude that settlements in the
Uruk expansion were not connected by regular exchange.
Table 1 – Comparative chronological table.
PeriodDate Northern Mesopotamia
BC
3100
3200
3300
3600
3900
4200
North Mesop.
South Mesop.
LC5
LC4
LC3
LC2
Late Uruk
MiddleUruk
EarlyUruk
Ubaid5
CentralMesopot.
SouthernMesopotamia
Iran
SusaAcropole IChoga MishGodin
TepeGeoy Tepe
Uruk EannaNippurHacinebi Habuba
KabiraSheikhHassan Tell Brak Tell
FeresTepe
GawraNinevehTell
Leilan Girdi Qala
17
19
2021
22
18
hiatus
(Suse A)23-27
Farukh
VI: 1
VI: 2
VI: 3
VIIIPhase
M
Prot
olite
rate
Term
inal
S
usa
Late
Sus
iana
II
IVA
IVBV
VI
VIIVIII
X
XIII
XV
XVI
XVIIXVIII
XIXXXI
hiatusTrench C
Level 1-7
Level 8-10
B2
B1
A
Late Uruk
Levels5-4
Levels8-6
Levels10-13
IV
V
hiatus
1A
1B1C
2A2B3
4A4B5
6
X-IX
VIII
XaXI
XIA-B
Nineveh IV-31-20
-37-31
-45-37
NordUruk B
NordUruk A
Gawra B Phase
-45
Gawra A Phase
-59
TW 11-10 Phase G
TW 14-13,CH 14-13 Phase F
TW 22-21(20)
CH 17a
TW 19-15,CH 16-15,
HS1 Phase F
TW 12 beginning
Ph. G
CH 17-18
XII
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82 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
focus is about to shift. In fact, the definition of ‘local’ and ‘for-
eign’ repertoires is not really useful without a stronger emphasis
on the local evolution of these traditions (and, therefore, of the
underlying groups of producers), with their conservatism,
hybridizations, specificities or technical borrowings. The discov-
ery of a major craft district at Girdi Qala is in itself a significant
element, since previously there was no direct information about
the structures and organization of ceramic production in the
Uruk colonial network for this phase. It raises the possibility of
studying relationships between local and South Mesopotamian
settlers in terms of pottery production, opening new perspectives
on economic and cultural practices of cooperation or segrega-
tion. Girdi Qala and Logardan have already provided and should
continue to provide in coming years startling new archaeological
evidence, re-opening the debate on the Uruk expansion and
interactions between Southern and Northern Mesopotamia.
ACKNOWLEDGMENTS
We would like to express our warmest thanks to our Kurdish part-
ners, the DGA in Erbil and above all to Kamal Rasheed and his team
of the Directorate of Antiquities of Sulaymaniyah, who invited us
to Kurdistan and whose continuous support was greatly appreciated
by all of us. We wish to thank Saber Ahmed Saber and Sami Jamil
Hamarasheed, who were from beginning to end precious collabo-
rators. We address also special thanks to Salah Salman Rumaiydh
(SBAH) and Shayban al Rawi (University of Ramadi). Both of them
visited the sites and gave us many useful advices. Finally, we are
pleased to thank the authorities of Chamchamal and Shosh for their
support, the people of Shorsh for their friendly welcome and, last but
not least, the 15 fine workers that we were able to recruit there.
Régis VALLETCNRS, IFPO
Head of the Iraq branch (Erbil)[email protected]
Johnny S. BALDIIFPO, Beyrouth – LEBANON
Hugo NACCAROUMR 7041 ArScAn-VEPMO
Maison Archéologie et Ethnologie92023 Nanterre cedex – FRANCE
Kamal RASHEEDDirector of Antiquities of the Sulaymaniyah Governorate
KRG – IRAQ [email protected]
Saber Ahmed SABER Sami Jamil HAMARASHEED
Directorate of Antiquities of SulaymaniyahKRG – IRAQ
BIBLIOGRAPHY
Abu Jayyab K.
2012 A ceramic chronology from Tell Hamoukar’s southern extention.
In: Marro C. (ed.): 87-128.
Akkermans P.M.M.G
1988 The Period V Pottery. In: Van Loon M.N. (ed.), Hammam et-Turkman I. Report of the University of Amsterdam Excavations in Syria I: 287-349. Istanbul: Nederlands Historisch-
Archeologisch Instituut te stanbul.
Algaze G.
1993 The Uruk World System. The Dynamics of Expansion of Early Mesopotamian Civilization. Chicago: University of Chicago.
1999 Trends in the Archaeological Development of the Upper Euphrates
Basin of South-eastern Anatolia during the Late Chalcolithic and
the Early Bronze age. In: del Olmo Lete G. and Montero
Fenollós J.-L. (eds.), Archaeology of the Upper Syrian Euphrates: The Tishrin Dam Area: 535-572. Barcelona: Ausa.
Al-Kountar S. and Reichel C.
2008 Tell el-Hurriyeh-Hamoukar. Studia Orontica 4: 20.
Alizadeh A.
1983 A Protoliterate Kiln from Chogha Mish. Iran 23: 39-50.
Bachmann F.
1998a Das keramische Inventar eines urukzeitlichen Gebäudes in Tell
Sheikh Hassan/ Syrien. In: Lebeau M. (ed.), About Subartu. Studies devoted to Upper Mesopotamia / À propos de Subartu. Études consacrées à la Haute Mésopotamie. Vol 1: Landscape, Archaeology, Settlement: 89-129. Turnhout: Brepols (Subartu 4,1).
1998b Ein ‘Habuba Kabira Süd Horizont’ am Tell Scheikh Hassan?
Mitteilungen der Deutschen Orient-Gesellschaft 130: 51-67.
Badler V.R.
2002 A Chronology of Uruk Artefacts from Godin Tepe in Central
Western Iran and Implications for the Interrelationships between
local and foreign cultures. In: Postgate J.N. (ed.): 79-110.
Baldi J.S.
2012a Tell Feres al-Sharqi in LC1-2 period. Serial production and
regionalisation of ceramic traditions: a perspective from a small
rural site. In: Marro C. (ed.): 129-162.
2012b Coba bowls, mass production and social change in Post-Ubaid
Times. In: Marro C. (ed.): 393-416.
2012c Identità tecniche e identità sociali a Tell Feres al-Sharqi tra fine
Ubaid e LC2. Alcune riflessioni ceramologiche sull’apparizione
del mestiere di vasaio nel nord della Mesopotamia tardo calcoli-
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 83
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
tica. In: Mazzoni S. (a cura di.), Studi di Archeologia del Vicino Oriente: scritti degli allievi fiorentini per Paolo Emilio Pecorella: 11-38. Firenze: Firenze University Press.
2013a Anthropological reading of the ceramics and emergence of a
profession: a protohistoric North-Mesopotamian view from Tell
Feres al-Sharqi. In: Anguiozar L.G., González M.L. y
Lopes M.C. (coord.), Actas del I Congreso Internacional sobre Estudios Cerámicos, Homenaje a la Dra. Mercedes Vegas – Cadiz, del 1 al 5 noviembre de 2010: 477-504. Cádiz: Universidad
de Cádiz.
2013b Ceramic Technology at Tell Qarassa North (Southern Syria):
From “Cultures” to “Ways of Doing”. In: Bombardieri L.,
D’Agostino A., Guarducci G., Orsi V. and Valentini S.
(eds.), Identity and Connectivity: Proceedings of the 16th Symposium on Mediterranean Archaeology, Florence, Italy, 1–3 March 2012. Vol. 1: Near Eastern Identities: 17-24. Oxford (BAR Int. Ser. 2581).
Baldi J.S. and Abu Jayyab K.
2012 A comparison of the ceramic assemblages from Tell Feres al-
Sharqi and Hamoukar. In: Marro C. (ed.): 163-182.
Balossi Restelli F.
2006 The local Late Chalcolithic (LC3) occupation at Zeytinli Bahçe
(Birecik, anli-Urfa): the ceramic production. Anatolian Studies
56: 17-46.
Boese J.
1995 Ausgrabungen in Tell Sheikh Hassan. Vorläufige Berichte über die Grabungskampagnen 1984-1990 und 1992-1994. Saar-
brücken: Saarbrücker Druckerei und Verlag (Schriften zur vor-derasiatischen Archäologie 5).
Butterlin P.
2003 Les temps proto-urbains de Mésopotamie. Contacts et accultu-ration à l’époque d’Uruk au Moyen-Orient. Paris : CNRS
Éditions.
Cauvin J. et Stordeur D.
1985 Une occupation d’époque Uruk en Palmyrène : le niveau supé-
rieur d’El Kowm 2 – Caracol. Cahiers de l’Euphrate 4 : 191-205.
Creekmore A.
2007 The Upper Tigris Archaeological Research Project (UTARP): A
Summary and Synthesis of the Late Chalcolithic and Early
Bronze Age Remains from the First Three Seasons at Kenan
Tepe. Anatolica 33: 75-127.
Delcroix G. et Huot J.-L.
1972 Les fours dits “de potier” dans l’Orient ancien. Syria 49 : 35-95.
Delougaz P. and Kantor H.J
1996 Chogha Mish. Vol. I: The First Five Season of Excavations, 1961-1971 (ed. by A. Alizadeh). Chicago: The Oriental Insti -
tute of the University of Chicago (OIP 101).
Eichmann R.
1989 Uruk, die Stratigraphie. Mainz am Rhein: Philipp von Zabern
(Ausgrabungen in Uruk-Warka Endberichte 3).
1991 Aspekte prähistorischer Grundrissgestaltung in Vorderasien: Beiträge zum Verständnis bestimmter Grundrissmerkmale in ausgewählten neolithischen und chalkolithischen Siedlungen des 9. - 4. Jahrtausends v. Chr. (mit Beispielen aus der euro-päischen Prähistorie). Mainz am Rhein: Philipp von Zabern.
2007 Uruk Architektur I. Von den Anfängen bis zur frühdynastischen Zeit. Rahden: Marie Leidorf (Ausgrabungen in Uruk-Warka Endberichte 14).
Emberling G. and Minc L.
2016 Ceramics and long-distance trade in early Mesopotamian states.
Journal of Archaeological Science: Reports 7: 819-834.
Fiorina P.
1997 Khirbet Hatara. La stratigrafia. Mesopotamia 27: 7-45.
2001 Khirbet Hatara. La ceramica del livello 1. Mesopotamia 36: 1-47.
Forest J.-D. and Vallet R.
2008 Urukian Architecture from Abroad: Some Thoughts about
Hassek Höyük. In: Cordoba J.M., Molist M., Pérez M.C.,
Rubio I. and Martinez S. (eds.), Proceedings of the 5th International Congress on the Archaeology of the Ancient Near East. Vol. II: 39-52. Madrid: UAM.
Forest J.-D., Vallet R. and Baldi J.S.
2012 Tell Feres al Sharqi: A 5th-4th millennium site in the Khabur
drainage basin. In: Matthews R. and Curtis J. (eds.),
Proceedings of the 7th International Congress on the Archaeology of the Ancient Near East 12 April – 16 April 2010, the British Museum and UCL, London. Vol. 3, Fieldwork & Recent Research: 33-50. Wiesbaden: Harrassowitz Verlag.
Forest J.-D., Vallet R., Baldi J.S. et Emery E.
2014 Tell Feres al Sharqi, synthèse provisoire au terme de trois cam-
pagnes (2006-2008). Annales Archéologiques Arabes Syriennes
53-54 : 15-58.
Frangipane M.
1993 Local Components in the Development of Centralized Societies
in Syro-Anatolian Regions. In: Frangipane M.,
Hauptmann H., Liverani M., Matthiae P. and
Mellink M. (eds.), Between the Rivers and over the Mountains: Archaeologica Anatolica et Mesopotamica Alba Palmieri Dedicata: 133-161. Roma: Università degli studi di Roma “La
Sapienza”.
1996 La nascita dello Stato nel Vicino Oriente. Dai lignaggi alla burocrazia nella grande Mesopotamia. Roma e Bari: Laterza.
2000 The Late Chalcolithic/EB I sequence at Arslantepe.
Chronological and cultural remarks from a frontier site. In:
Marro C. et Hauptmann H. (éd.): 439-471.
2001 Centralization Processes in Greater Mesopotamia. Uruk
“Expansion” as the Climax of Systemic Interactions among
Areas of the Greater Mesopotamian Region. In: Rothman M.S.
(ed.): 307-347.
2002 Non-Uruk developments and Uruk-linked features. In:
Postgate J.N. (ed.): 123-148.
2009 Non-Urban Hierarchical Patterns of Territorial and Political
Organization in Northern Regions of Greater Mesopotamia:
Tepe Gawra and Arslantepe. In: Butterlin P. (éd.), À propos de Tepe Gawra, le monde proto-urbain de Mésopotamie. About Tepe Gawra. A Proto-Urban World in Mesopotamia : 135-148.
Turnhout : Brepols (Subartu 23).
2010 Different Models of Power Structuring at the Rise of Hierarchical
Societies in the Near East: Primary Economy versus Luxury and
Defense Management. In: Bolger D. and Maguire L.C. (eds.),
The Development of Pre-State Communities in the Ancient Near East. Studies in Honour of Edgar Peltenburg: 79-86. Oxford and
Oakville: Oxbow Books (BANEA Publication Series 2).
Gavagnin K., Iamoni M. and Palermo R.
2016 The Land of Nineveh Archaeological Project: The Ceramic
Repertoire from The Early Pottery Neolithic to the Sasanian
Period. Bulletin of the American Schools of Oriental Research 375: 119-169.
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
84 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
Gelbert A.
2003 Traditions céramiques et emprunts techniques dans la vallée du fleuve Sénégal. Ceramic Traditions and Technical Borrowings in the Senegal Valley. Paris : Éditions de la Maison des Sciences
de l’Homme.
Gopnik H. and Rothman M.S.
2011 On the High Road. The History of Godin Tepe, Iran. Costa Mesa,
CA: Mazda Publishers; Royal Ontario Museum (Bibliotheca Iranica: Art, Archaeology and Architecture Ser. 1).
Gosselain O. P.
2002 Poteries du Cameroun méridional. Styles techniques et rapports à l’identité. Paris : CNRS Éditions (CRA, Monographie 26).
2008 Mother Bella was not a Bella. Inherited and transformed tradi-
tions in Southwestern Niger. In: Stark M.T., Bowser B. and
Horne L. (eds.), Cultural Transmission and Material Culture. Breaking Down Boundaries: 150-177. Tucson: The University of
Arizona Press.
Goulder J.
2010 Administrator’s bread: an experiment-based re-assessment of the
functional and cultural role of the Uruk bevel-rim bowl. Antiquity
84,324: 351-362.
Gut R.
1995 Das prähistorische Ninive. Zur relativen Chronologie der frühen Perioden Nordmesopotamiens. Mainz am Rhein: Philipp von
Zabern (Baghdader Forschungen 19).
2002 The Significance of the Uruk Sequence at Nineveh. In:
Postgate J.N. (ed.): 17-48.
Habibi A. and Karami M.
2008-2009 Uruk Pottery, based on strip survey of south Abu Fandowah site,
Khuzestan, south-western Iran. Payam-e Bastanshenas 5,10:
66-92.
Hansen Streily A.
2000 Early Pottery Kilns in the Middle East. Paléorient 26,2: 69-81.
Hauptmann H.
1972 Die Grabungen auf dem Norsün Tepe, 1970. In: Keban Project 1970 Activities: 103-117. Ankara: Middle East Technical
University (Keban Project Publications I.3).
1976 Die Grabungen auf dem Norsün Tepe, 1972. In: Keban Project 1972 Activities: 71-90. Ankara: Middle East Technical University
(Keban Project Publications I.5).
1979 Die Grabungen auf dem Norsün Tepe, 1973. In: Keban Project 1973 Activities: 61-78. Ankara: Middle East Technical University
(Keban Project Publications I.6).
1982 Die Grabungen auf dem Norsün Tepe, 1974. In: Keban Project 1974-1975 Activities: 41-70. Ankara: Middle East Technical
University (Keban Project Publications I.7).
Helwing B.
2000 Regional variation in the composition of Late Chalcolithic pot-
tery assemblages. In: Marro C. et Hauptmann H. (éd.) : 145-
164.
2002 Hassek Höyük II. Die Spätchalkolithische Keramik. Tübingen:
E. Wasmuth (Istanbuler Forschungen 45).
Huot J.-L. et Vallet R.
1990 Les habitations à salles hypostyles d’époque Obeid 0 de Tell el
‘Oueili. Paléorient 16,1 : 125-130.
Kepinski C.
2011 New Evidence from Grai Resh, Northern Iraq, the 2001 and 2002
seasons. A pre-Uruk expansion site from the Late Chalcolithic
Period. Zeitschrift für Orient-Archäologie 4: 26-81.
Killick R.G., Cuyler Young T., Watson P.J., Payne S., Downs D., McAdam E., Mynors H.S., Miller R., Crawford H.E.W., Moon J.A. and Arnold K.
1988 Tell Rubeidheh. An Uruk Village in the Jebel Hamrin.
Warminster: British School of Archaeology in Iraq, Aris and
Phillips (Iraq Archaeological Reports 2; Hamrin Salvage Project Report 7).
Kingery W.D.
1997 Operation Principles of Ceramic Kilns. In: Rice P.M and
Kingery W.D. (eds.), The Prehistory and History of Ceramic Kilns: 11-19. Westerville: Wiley, American Ceramic Society
(Ceramics and Civilization Series 7).
Kopanias K. and MacGinnis J. (eds.)
2016 The Archaeology of the Kurdistan Region of Iraq and Adjacent Regions. Oxford: Archaeopress.
Le Brun A.
1971 Recherches stratigraphiques à l’Acropole de Suse, 1969-1971.
Cahiers de la Délégation Archéologique Française en Iran 1 :
163-233.
1978a La glyptique du niveau 17B de l’Acropole (campagne 1972).
Cahiers de la Délégation Archéologique Française en Iran 8 :
61-79.
1978b Suse, chantier « Acropole 1 ». Paléorient 4 : 177-192.
Leroi Gourhan A.
1945 Évolution et techniques. Milieu et techniques. Paris : Albin
Michel.
Lloyd S.
1938 Some Ancient Sites in the Sinjar District. Iraq 5,2: 123-142.
1940 Iraq Government Soundings at Sinjar. Iraq 7,1: 13-21.
Majidzadeh Y.
1977 The Development of the pottery kiln in Iran from Prehistoric to
Historical Periods. Paléorient 3: 207-221.
Marro C.
2010 Where did Late Chalcolithic Chaff-Faced Ware originate?
Cultural Dynamics in Anatolia and Transcaucasia at the Dawn
of the Urban Civilization (ca 4500-3500 BC). Paléorient 36,2:
35-55.
Marro C. (ed.)
2012 After the Ubaid. Interpreting Change from the Caucasus to Mesopotamia at the Dawn of Urban Civilization (4500-3500 BC). Papers from The Post-Ubaid Horizon in the Fertile Crescent and Beyond. International Workshop held at Fosseuse, 29th June-1st July 2009. Istanbul, Paris: De Boccard (Varia Anatolica 27).
Marro C. et Hauptmann H. (éd.)
2000 Chronologies des pays du Caucase et de l’Euphrate aux IVe-IIIe millénaires / From the Euphrates to the Caucasus: Chronologies for the 4th-3rd Millennium B.C. Actes du colloque d’Istanbul, 16-19 décembre 1998. Istanbul, Paris : IFEA, De Boccard (Varia Anatolica 11).
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 85
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
Matthews R.
2003 Excavations at Tell Brak. Vol. 4: Exploring an Upper Meso-potamian Regional Centre, 1994-1996. Cambridge: McDonald
Institute for Archaeological Research.
Minc L. and Emberling G.
2016 Trade and interaction during the era of the Uruk expansion:
Recent insights from archaeometric analyses. Journal of Archaeological Science: Reports 7: 793-797.
Moorey P.R.S.
1994 Ancient Mesopotamian Materials and Industries. The Archaeological Evidence. New York: Oxford University Press.
Nissen H.
2002 Uruk: Key Site of the Period and Key Site of the Problem. In:
Postgate J.N. (ed.): 1-16.
Nöldeke A.
1937 Achter vorläufiger Bericht über die von der Deutschen Forschungsgemeinschaft in Uruk-Warka unternommenen Ausgrabungen. Berlin: Verlag der Akademie der Wissenschaften.
Numoto H.
1987 Tell Musharifa. In: Fujii H. (ed.), Working Report on First
Season of Japanese Archaeological Excavation in Saddam Dam
Salvage Project. In: Researches on the Antiquities of Saddam Dam Basin Salvage and Other Researches: 49-54. Baghdad:
State Organisation of Antiquities and Heritage.
Oates D. and Oates J.
1993 Excavations at Tell Brak 1992-1993. Iraq 55: 155-199.
Oates J.
1985 Tell Brak: Uruk pottery from 1984 season. Iraq 47: 175-186.
1986 Tell Brak: The Uruk/Early Dynastic Sequence. In:
Finkbeiner U. and Röllig W. (eds.), amdat Nasr. Period or Regional Style?: 245-273. Wiesbaden: Dr. Ludwig Reichert
(Beihefte zum Tübinger Atlas des Vorderen Orients B 62).
1987 A note on the ‘Ubaid and Mitanni Pottery from Tell Brak. Iraq
49: 193-198.
Oates J., McMahon A., Karsgaard P., al-Quntar S. and Ur J.
2007 Early Mesopotamian urbanism: A new view from the north.
Antiquity 81,313: 585-600.
Orton C.R.
1993 How many pots make five? An historical review of pottery quan-
tification. Archaeometry 35,2: 169-184.
Özguç N.
1992 The Uruk Culture at Samsat. In: Hrouda B., Kroll S. und
Spanos P.Z. (Hrsg.), Von Uruk nach Tuttul. Eine Festschrift für Eva Strommenger: 151-157. München, Wien: Profil Verlag.
Patton J.Q.
2008 Learning and transmission of pottery style. Women’s life histo-
ries and communities of practice in the Ecuadorian Amazon. In: Stark M., Bowser B.J. and Horne L. (eds.), Cultural Transmission and Material Culture. Breaking down Boundaries: 105-129. Tucson: The University of Arizona Press.
Pearce J.
2000 The Late Chalcolithic sequence at Hacınebi Tepe, Turkey. In:
Marro C. et Hauptmann H. (éd.) : 115-144.
Pollock S. and Coursey C.
1995 Ceramics from Hacınebi Tepe: Chronology and Connections.
Anatolica 21: 101-141.
1996 Hacınebi Uruk Pottery: Preliminary Report. In: Stein G.J. et al., Uruk Colonies and Anatolian Communities: An Interim
Report on the 1992-1993 Excavations at Hacınebi, Turkey.
American Journal of Archaeology 100,2: 205-260.
Pool C.A.
2000 Why a kiln? Firing technology in the Sierra de los Tuxtlas,
Veracruz (Mexico). Archaeometry 42,1: 61-76.
Postgate J.N. (ed.)
2002 Artefacts of Complexity: Tracking the Uruk in the Near East. Warminster: Aris and Phillips, British School of Archaeology in
Iraq (Iraq Archaeological Reports 5).
Postgate J.N. and Moon J.A.
1982 Excavations at Abu Salabikh, 1981. Iraq 44,2: 103-136.
Reichel C.D.
2009 Hamoukar. In: Stein G.J. (ed.), Oriental Institute 2008-2009 Annual Report: 77-87. Mattoon, IL: United Graphics Incor-
porated.
Reimer S.
1989 Tell Qraya on the Middle Euphrates. In: Rothman M.S. (ed.),
“Out of the Heartland: The Evolution of Complexity in Peripheral
Mesopotamia during the Uruk Period”, Workshop Summary.
Paléorient 15,1: 284.
Rothman M.S.
1993 Another Look at the “Uruk Expansion” from the Tigris Piedmont.
In: Frangipane M., Hauptmann H., Liverani M.,
Matthiae P. and Mellink M. (eds.), Between the Rivers and over the Mountains: Archaeologica Anatolica et Mesopotamica Alba Palmieri Dedicata: 162-176. Roma: Università degli studi
di Roma “La Sapienza”.
2002 Tepe Gawra: The Evolution of a Small Prehistoric Center in Northern Iraq. Philadelphia: University of Pennsylvania,
Museum of Archaeology and Anthropology (Museum Monographs 112).
Rothman M.S. (ed.)
2001 Uruk Mesopotamia and Its Neighbors. Cross-Cultural Interaction in the Era of State Formation. Santa Fe: School of
American Research (School of American Research Advanced Seminar Series).
Rothman M.S and Badler V.R.
2011 Contact and Development in Godin Period VI. In: Gopnik H.
and Rothman M.S. (eds.), On the High Road. The History of Godin Tepe, Iran: 67-137. Costa Mesa, CA: Mazda Publishers,
Royal Ontario Museum (Bibliotheca Iranica: Art, Archaeology and Architecture Series 1).
Rothman M.S and Peasnall B.
1999 Societal Evolution of Small, Pre-state Centers and Polities: The
example of Tepe Gawra in Northern Mesopotamia. Paléorient 25,1: 101-114.
Roux V.
2010 Lecture anthropologique des assemblages céramiques.
Fondements et mise en œuvre de l’analyse technologique. Les Nouvelles de l’archéologie 119 : 4-9.
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
86 R. Vallet, J.S. Baldi, H. Naccaro, K. Rasheed, S.A. Saber and S.J. Hamarasheed
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
Roux V. and Courty M.-A.
2005 Identifying social entities at a macro-regional level: Chalcolithic
ceramics of South Levant as a case study. In: Livingstone-
Smith A., Bosquet D. and Martineau R. (eds.), Pottery Manufacturing Processes: Reconstruction and Interpretation. Actes du XIVe congrès de l’IUSPP, Liège, 2001: 201-214. Oxford
(BAR Int. Ser. 1349).
2007 Analyse techno-pétrographique céramique et interprétation fonc-
tionnelle des sites : un exemple d’application dans le Levant Sud
chalcolithique. In: Bain A., Chabot J. et Moussette M. (éd.),
La mesure du passé : contributions à la recherche en archéomé-trie (2000-2006) : 153-167. Oxford (BAR Int. Ser. 1700).
Rova E.
1999-2000 A tentative Synchronization of the Local Late Chalcolithic
Ceramic Horizons of Northern Syro-Mesopotamia. Mesopotamia 34-35: 175-199.
2007 The Late Chalcolithic Period in the Tell Leilan Region: a Report
on the Ceramic Material of the 1995 Survey. Kaskal 4: 1-42.
Schwartz G.M.
1988 A Ceramic Chronology from Tell Leilan: Operation 1. New Haven and London: Yale University Press (Tell Leilan Research 1).
Stark M.T.
1998 The Archaeology of Social Boundaries. Washington, DC:
Smithsonian Institution Press.
Stark M.T., Bowser B.J. and Horne L. (eds.)
2008 Cultural Transmission and Material Culture. Breaking Down Boundaries. Tucson: Arizona University Press.
Starr R.
1937-39 Nuzi: Report on the Excavations at Yorgan Tepa near Kirkuk, Iraq, 1927-1931 (vol. I-II). Cambridge, Mass.: Harvard
University Press.
Stein G.J.
1998 World Systems Theory and Alternative Modes of Interaction in
the Archaeology of Culture Contact. In: Cusick J.G. (ed.),
Studies in Culture Contact: Interaction, Culture Change, and Archaeology: 220-255. Carbondale: Center for Archaeological
Investigations, Southern Illinois University Press (Occasional Paper 25).
1999 Rethinking World-Systems: Diasporas, Colonies and Interaction in Uruk Mesopotamia. Tucson: University of Arizona Press.
2001 Indigenous Social Complexity at Hacınebi (Turkey) and the
Organization of Uruk Colonial Contact. In: Rothman M.S.
(ed.): 265-306.
2002a The Uruk Expansion in Anatolia: A Mesopotamian colony and
its indigenous host community at Hacınebi, Turkey. In:
Postgate J.N. (ed.): 149-171.
2002b From passive periphery to active agents: emerging perspectives
in the archaeology of interregional interaction. American Anthropologist 104,3: 903-916.
Stephen F. and Peltenburg E.
2002 Scientific analysis of Uruk Ceramics from Jarablus Tahtani and
other Middle-Upper Euphrates sites. In: Postgate J.N. (ed.):
173-190.
Strommenger E., Sürenhagen D. und Rittig D.
1980 Habuba Kabira: Eine Stadt vor 5000 Jahren. Ausgrabungen der Deutschen Orient Gesellschaft am Euphrat in Habuba Kabira, Syrien. Mainz am Rhein: Philipp von Zabern.
Strommenger E., Sürenhagen D. and Rittig D.
2014 Die Kleinfunde von Habuba Kabira-Süd. Wiesbaden:
Harrassowitz (Wissenschaftliche Veröffentlichungen der Deutschen Orient-Gesellschaft 141).
Suleiman A. and Nieuwenhuyse O.
2002 The Late Chalcolithic Occupation. In: Suleiman A. and
Nieuwenhuyse O. (eds.), Tell Boueid II: A Late Neolithic Village on the Middle Khabur (Syria): 153-169. Turnhout:
Brepols (Subartu 11).
Sürenhagen D.
1979 Ahmad al-Hattu 1978. Mitteilungen der Deutschen Orient-Gesellschaft 111: 35-50.
Vallet R.
1990 Les habitations à salles hypostyles des débuts de l’époque
d’Obeid. Comptes rendus de l’Académie des Inscriptions et Belles-Lettres 1990/4 : 867-874.
1996 L’architecture des phases Obeid 0 et 1. Travaux de 1989. In : Huot J.-L. (éd.), Oueili. Travaux de 1987 et 1989 : 103-139.
Paris : ERC.
1997a Habuba Kébira sud, approche morphologique de l’habitat. In : Castel C., Al-Maqdissi M., Villeneuve F. (éd.), La maison dans la Syrie antique du IIIe millénaire au début de l’Islam. Pratiques et représentations de l’espace domestique. Actes du Colloque International, Damas 27-30 juin 1992 : 105-119.
Beyrouth : IFAPO (BAH 150).
1997b Habuba Kébira ou la naissance de l’urbanisme. Paléorient 22,2 :
45-76.
1998 L’urbanisme colonial urukien, l’exemple de Djébel Aruda. In:
Lebeau M. (ed.), About Subartu. Studies devoted to Upper Mesopotamia. Vol. 1: Landscape, Archaeology, Settlement: 53-87. Turnhout: Brepols (Subartu 4,1).
2014 Tell Feres al Sharki 2010: Recent Discoveries on the Ubaid and
Late Chalcolithic in North Syria. In: Bielinski P., Gawlikowski M. and Kolinski R. (eds.), Proceedings of the 8th International Congress on the Archaeology of the Ancient Near East, 30 Avril – 4 Mai 2012, Warsaw: 271-287. Wiesbaden:
Harrassowitz.
In press Tell Feres, a failed pathway towards urbanism in Northern
Mesopotamia. In: Masetti-Rouault M.-G. (ed.), Archaeology and History of Empires: Models, projects and work in progress in Northern Mesopotamia. New programs in Iraqi Kurdistan,
Proceedings of the École Pratique des Hautes Études International Congress, Paris, 14-15 juin 2013. Turnhout:
Brepols (EMMS 1).
Vallet R. and Baldi J.S.
2016 Tell Feres: New Evidence on the Development of Proto-Urban
Societies in Northern Mesopotamia. In: Kanjou Y. and
Tsuneki A. (eds.), A History of Syria in One Hundred Sites:
91-97. Oxford: Archaeopress.
Van Driel G.
1980 The Uruk Settlement on Jebel Aruda: A Preliminary Report. In:
Margueron J.-C. (éd.), Le Moyen Euphrate. Zone de contacts et d’échanges. Actes du colloque de Strasbourg, 10-12 mars 1977 : 73-93. Leiden : E.J. Brill (Travaux du Centre de recherches sur le Proche-Orient 5).
Van Driel G. and Van Driel-Murray C.
1979 Jebel Aruda 1977-1978. Akkadica 12: 2-28.
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
New evidence on Uruk expansion in the Central Mesopotamian Zagros Piedmont 87
Paléorient, vol. 43.1, p. 61-87 © CNRS ÉDITIONS 2017
1983 Jebel Aruda, the 1982 season excavation, interim report.
Akkadica 33: 1-26.
Veit U.
1994 Ethnic concepts in German prehistory: a case-study on the rela-
tionship between cultural identity and archaeological objectivity.
In: Shennan S.J. (ed.), Archaeological Approaches to Cultural Identity: 35-56. London and New York: Routledge (One World Archaeology 10).
Wallaert H.
2001 Mains agiles, mains d’argile. Apprentissage de la poterie au Nord-Cameroun : modes d’acquisition of comportements tech-niques. Thèse de doctorat non publiée. Université Libre de
Bruxelles.
2008 The way of the potter’s mother. Apprenticeship strategies among
Dii potters from Cameroon, West Africa. In: Stark M.T.,
Bowser B.J. and Horne L. (eds.), Cultural Transmission and Material Culture: Breaking Down Boundaries: 178-198. Tucson:
The University of Arizona Press.
Wallerstein I.
1974 The Modern World-System, vol. I: Capitalist Agriculture and the Origins of the European World-Economy in the Sixteenth Century. New York and London: Academic Press.
1980 The Modern World-System, vol. II: Mercantilism and the Consolidation of the European World-Economy, 1600-1750.
New York and London: Academic Press.
Welsch R.L. and Terrell J.E.
1998 Material culture, social fields and social boundaries on the Sepik
Coast of New Guinea. In: Stark M.T. (ed.), The Archaeology of Social Boundaries: 50-78. Washington, DC: Smithsonian
Institution Press.
Wilhelm G. and Zaccagnini C.
1993 Tell Karrana 3, Tell Jikan, Tell Khirbet Salih. Mainz am Rhein:
Philipp Von Zabern (Baghdader Forschungen Band 15).
Wright H.T.
2014 Early Uruk Ceramic Assemblages: Cultural Relations in Greater
Mesopotamia During the Late Fifth and Early Fourth Millennia
BC. In: McMahon A. and Crawford H. (eds.), Preludes to Urbanism. The Late Chalcolithic of Mesopotamia. In Honour of Joan Oates: 109-125. Cambridge: University of Cambridge
(McDonald Institute for Archaeological Research).
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT
CN
RS
ÉD
ITIO
NS
- TI
RÉ
S À
PA
RT